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Photo from Glen Canyon National Recreation Area, Utah.

From top to bottom: Rounded tan domes of the Navajo Sandstone, layered red Kayenta Formation, cliff-forming, vertically jointed, red Wingate Sandstone, slope-forming, purplish Chinle Formation, layered, lighter-red Moenkopi Formation, and white, layered Cutler Formation sandstone.

The lower sandstone layer is disrupted by two faults, so we can infer that the faults are younger than that layer.

But the faults do not appear to continue into the coal seam, and they certainly do not continue into the upper sandstone.

The lava flow took place some time after the diorite cooled, was uplifted, and then eroded.

(Hammerhead for scale) [SE]Figure 8.6b Rip-up clasts of shale embedded in Gabriola Formation sandstone, Gabriola Island, B. The pieces of shale were eroded as the sandstone was deposited, so the shale is older than the sandstone.

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